• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.159-160
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• 2002

도시가 개발됨에 따라 녹지 등의 자연지면이 포장지면으로 바뀌고, 대량의 열과 오염물질이 대기중으로 배출되고 있다. 그 결과 도시는 주변지역보다 온도가 높은 고온화 현상, 풍속의 감소와 함께 운량, 안개일수, 강수량의 변화, 지표면의 증발량 감소에 의한 상대습도의 저하 등의 도시의 고유한 기후특성을 가진다. 이러한 도시의 기후특성 중 가장 뚜렷한 특징은 기온의 고온화현상이다. (중략)

• Proceedings of the Korean Association of Geographic Inforamtion Studies Conference
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• 2010.09a
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• pp.384-386
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• 2010

본 연구의 목적은 도시고온화와 도시열섬 현황을 파악하는데 있어 중요한 역할을 하는 도시 지역의 알베도와 지표면의 토지이용 자료를 이용하여 한반도 행정구역의 알베도 분포를 비교 평가하고자 하는 것이다. 도시 지역의 알베도와 토지이용을 현장조사 할 경우 많은 시간과 비용이 소요되기 때문에, 시간적 경제적인 비용절감효과를 위해 전 지구적으로 변화를 감지할 수 있도록 NASA에서 제공하는 MODIS 위성영상 자료를 사용하여 분석하였으며, 그 결과 서울, 부산, 대구 등 주요 도시를 중심으로 대체적인 알에도 값이 낮게 나타났다. 이는 도시 지역의 인공 환경의 영향으로 인하여 주요 도시 지역이 주변 지역보다 알베도 수치가 낮게 나타났음을 알 수 있고 이러한 알베도 수치는 도시 열환경에 직접적인 영향을 주고 있으며 따라서 도시고온화와 도시열섬 현상을 감소시키기 위하여 도시 내 빌딩 및 도로의 재질개선, 지붕 및 도로 포장, 건물의 외벽을 밝은 색으로 교체 등의 방법으로 지표면 알베도를 높이기 위한 방안 마련이 시급 할 것이다.

• Proceedings of the Korea Water Resources Association Conference
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• 2016.05a
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• pp.319-319
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• 2016

최근 급격한 기후변화와 도시화로 인하여 강우량 및 강우강도는 약 20% 증가하고 강우일수는 14% 감소하며 도시 기온이 최대 $3^{\circ}C$까지 증가하는 등의 현실적인 문제가 발생하고 있다. 이로 인한 도시 물순환체계의 파괴는 도시물관리 여건의 악화로 이어지고 특히 불투수면적 증가로 인한 도시 홍수 및 침수의 증가, 잦은 도시 고온 현상, 도시하천의 건천화로 수질 악화를 야기하는 실정이다. 이에 국토의 자연자원을 보전하고 기후변화에 적응하면서 도시의 안전도와 가치를 높이기 위한 물관리 정책은 먼저 물을 순환을 보다 적극적으로 반영하고 통합적인 물관리 체계 확보를 요구한다. 이를 위해서는 발생원 관리를 포함한 소규모 분산관리 체계로 변화하여야 하며 이들 시설에 대한 네트워크화를 통해 기후변화에 강건하고 통합관리쳬계를 구축하는 것이 중요하다. 이를 위해서는 저영향개발(LID, Low Impact Development) 및 그린인프라(GI, Green Infrastructure) 기반의 분산식 빗물관리기법의 도입이 절실하다. 현재 국내에서는 제도적으로 기후변화 대비, 지속가능한 도시환경 구축을 위한 물순환 건전화를 위해 100대 국정화제에 포함시키는 등(2013.2) 도시계획 및 기반시설 설치 LID기법의 법제적 산업적 도입을 추진중에 있으나, LID 기술의 수자원 치수, 이수 및 환경 효율성에 대한 객관적인 정보의 부재, LID 기술에 대한 효율성 검증 및 인증시스템의 부재, LID 기술의 무분별한 국외기술 도입으로 인한 효과 저감, LID 기술의 설계, 시공, 관리를 위한 매뉴얼 및 가이드라인의 부재, LID 기술에 대한 지자체 지원 및 전문가 양성 시스템의 부재 등 복합적인 문제를 안고 있어 GI 및 LID 기술의 적용을 통한 새로운 도시 및 유역차원의 수자원확보와 재해경감기술 패러다임 확보가 용이하지 않다. 이를 위해 본 연구에서는 강우유출수 관리를 위한 LID기술 신뢰도 향상 및 단일화, 표준화된 효율성 검증 기술 개발과 더 나아가서 도시-건축-수자원-도로-조경 등의 종합적인 인프라를 바탕으로 LID기술 통합관리 및 기술 고도화를 위해 부산대학교 GI LID 물순환 실증단지의 계획 및 구축을 수행하였다.

• Journal of the Korean Institute of Landscape Architecture
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• v.39 no.3
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• pp.107-116
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• 2011

One of the major factors which increase urban temperature is roads. This paper is aimed to investigate the effect of urban roadside vegetation on the road surface temperature. For this, surface temperature was measured at 18 spots using the thermal imaging camera in terms of road components including use of roadside land use, roadway, sidewalk, roadside vegetation and vegetation median barrier. The size of the roadside vegetation and related urban road characteristics were also measured. In terms of the effect of roadside vegetation on a decrease in road surface temperature, the roadside land use as a green area or open space was the highest, followed by the size of vegetation median barrier and the size of roadside vegetation. Besides road surroundings, an increase in the green zone such as roadside vegetation and median strip vegetation has a significant impact on lowering road surface temperature. Therefore, a good solution for reducing urban heat island effects would be to increase the area of roadside vegetation and green areas along roads.

• 한국태양에너지학회:학술대회논문집
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• 2009.11a
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• pp.26-31
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• 2009

This study was analysed influence of urban higher temperature in Busan about time series analysis of AWS data. The results are as follows. (1) The temperature of Busan show min $13.2^{\circ}C$ ~max $15.8^{\circ}C$ by 50 years, it is on the rise. (2) The seasonal adjustment series, summer appeared min $17.5^{\circ}C$ ~max $28.9^{\circ}C$ with primitive series similarly. The winter was min $-11.4^{\circ}C$ ~max $17.9^{\circ}C$, the minimum temperature was more lowly than primitive series and maximum temperature was more higher than primitive series. The results, seasonal adjustment series is guessed with influence difference urban structural element beside seasonal factor. (3) Regional analytical result, January appeared with range of min 28% ~max 196% of the seasonal factor and August appeared min 90% ~ max 106%. One of the case which is of 100% or more of the seasonal factor January 12nd~17th, August appears at the 15~17th.

• Journal of the Korean Solar Energy Society
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• v.28 no.2
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• pp.19-27
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• 2008

This study aims at examining the correlation between air temperature and urban structure such as land cover. For this, it measured summer air temperature by using data log type thermometer installed the inside of instrument screen, in the 9 points of elementary school in Haeundae, Busan. The accomplished results of this study are followings. 1) As altitude goes up 100m, air temperature drops to $0.6{\sim}1.0^{\circ}C$. 2) As building coverage ratio increases 10%, air temperature increases $0.3{\sim}0.4^{\circ}C$. 3) As floor space index increases 100%, air temperature increases $0.4{\sim}0.5^{\circ}C$. 4) As artificial coverage ratio increases 10%, air temperature increases $0.1{\sim}0.2^{\circ}C$. 5) As natural coverage ratio increases 10%, air temperature decreases $0.1{\sim}0.2^{\circ}C$.

• Journal of Korean Society of Environmental Engineers
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• v.35 no.6
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• pp.422-429
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• 2013

It is generally known that the increase of the Earth surface temperature due to the global warming together with the land desertification by rapid urban development has caused severe climate and weather change. In desert or desertification land, it is observed that there are always severe flooding phenomena, even if desert sand has the high porosity, which could be believed as the favorable condition of rain water infiltration into ground water. The high runoff feature causes possibly another heavy rain by quick evaporation with the depletion of underground water due to the lack of infiltration. The basic physics of desert flooding is reasonably assumed due to the thermal buoyancy of the higher temperature of the soil temperature than that of the rain drop. Considering the importance of this topic associated with water resource management and climate disaster prevention, no systematic investigation has, however, been reported in literature. In this study, therefore, a laboratory scale experiment together with the effort of numerical calculation have been performed to evaluate quantitatively the basic hypothesis of run-off mechanism caused by the increase of soil temperature. To this end, first, of all, a series of experiment has been made repeatedly with the change of soil temperature with well-sorted coarse sand having porosity of 35% and particle diameter, 2.0 mm. In specific, in case 1, the ground surface temperature was kept at $15^{\circ}C$, while in case 2 that was high enough at $70^{\circ}C$. The temperature of $70^{\circ}C$ was tested as this try since the informal measured surface temperature of black sand in California's Coachella Valley up to at 191 deg. $^{\circ}F$ ($88^{\circ}C$). Based on the experimental study, it is observed that the amount of runoff at $70^{\circ}C$ was higher more than 5% compared to that at $15^{\circ}C$. Further, the relative amount of infiltration by the decrease of the surface temperature from 70 to $15^{\circ}C$ is about more than 30%. The result of numerical calculation performed was well agreed with the experimental data, that is, the increase of runoff in calculation as 4.6%. Doing this successfully, a basic but important research could be made in the near future for the more complex and advanced topic for this topic.

• Economic and Environmental Geology
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• v.53 no.6
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• pp.677-685
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• 2020

The host rock of the Usuki Stone Buddha Statues is dark gray welded tuff involved the Aso-4 pyroclastic flow sediments. This Buddha Statues are processing chlorosis from rainfall flowing above and underground water which were urgently needed for conservation measurement. White precipitates, the main source of salt weathering, on the surface of the Buddha Statues are mainly consisted of thenardite, gypsum and dolomite. Extraction experiment result shows that thenardite was dissolved at the beginning of stirring and then redissolved after 4 hours, and gypsum was detected until stirring for 2 hours, and then dissolved after stirring for 4 hours. As a result of monitoring the microclimate environment for 11 months to determine the recrystallization environment of white precipitates, the phase transition between thenadite and mirabilite appears widely in spring, and is maintained in an aqueous solution due to high temperatures in summer and fall. In winter, mirabilite is shown the widest by decreasing temperature. Therefore we requires details monitoring for blocking water transfer port and solved humidity environment in shelter.

• Korean Journal of Environmental Agriculture
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• v.28 no.1
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• pp.1-8
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• 2009

This study was aimed at assess environmental conservation functions by analyzing the change of land use areas in agricultural fields between 1999 and 2006, and comparing land surface temperature distribution between 1994 and 2006 in Yongin city. Land use maps of Yongin city were obtained from soil maps for 1999, Quickbird satellite images(less than 1 m) and parcel map for 2006. The land use area for Yongin city was in the order of forest > paddy field > upland > residence & building in 1999, and forest > residence & building > paddy field > upland in 2006. Decrease of paddy and upland fields reduced 34% and 41% of the capability of agricultural multifunctionality as to environment including flood control, groundwater recharge, and air cooling. Land surface temperature(LST) was derived from Landsat TM thermal infrared band acquired in September of 1994 and 2006 and classified into three grades. The results impplied that green vegetation in agricultural field and forest play an important role to reduce land surface temperature in warm season.